摘要
甘肃北山地区红山铁矿床为赋存于元古界青白口系顶部的沉积变质型铁矿床,其铁矿石主要类型为磁铁矿,少量为赤铁矿、镜铁矿。矿石储量可达亿吨,经野外调研和室内综合研究,本矿床形成于裂陷海盆中,与多处含铁的热卤水喷流柱上涌有关,属于"Sedex"型铁矿类型。
Honshan iron deposit in Beishan region of Gansu Province is a sedimentary metamorphic iron deposit occurred at the top of Proteroroic Qinbaikou System,its reserves shoul be above 0.1 billion tones.The iron ore consist of magnetite mainly with some hematite and iron glance.The results of field investigation and office study show that this deposit formed within rifted and depressed ocean basin,and it should be Sedex type iron deposit related with the eruption column of hot brine fluid.
出处
《甘肃地质》
2010年第3期9-18,共10页
Gansu Geology
关键词
红山铁矿床
成矿机制
“Sedex”型
甘肃北山
Hongshan iron deposit
metallogenetic mechanism
Sedex type
Beishan region of Gansu Province
